Anisotropic H-k stacking and (revisited) crustal structure in the southeastern margin of Tibet

P receiver functions (PRFs) and the H-k stacking technique are tools often used to constrain the thickness of the crust and the ratio between the velocities of P and S waves. Both the crustal depth and the Poisson's ratio are very important parameters to study the tectonic evolution of the lithosphere, but they can be significantly affected by the presence of crustal anisotropy. In order to address this problem, we have extended the isotropic...